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    The Structure of the Two-Dimensional Internal Boundary Layer over a Sudden Change of Surface Roughness

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 003::page 738
    Author:
    Rao, K. S.
    ,
    Wyngaard, J. C.
    ,
    Coté, O. R.
    DOI: 10.1175/1520-0469(1974)031<0738:TSOTTD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The effects of an abrupt change of surface roughness on the mean flow and turbulence structure in the neutral surface layer are numerically investigated by a higher-order turbulence closure theory, which includes dynamical equations for Reynolds stresses and the viscous dissipation rate. The closed system of governing equations, together with the specified initial and boundary conditions, is solved by an explicit finite-difference method on a digital computer. The numerical model predicts the distributions of mean wind, shear stress, turbulent energy and other quantities, with no a priori assumptions regarding the distributions of any of these variables in the transition region. The distributions of the nondimensional wind shear, the dissipation and mixing length scales, and the ratio of stress to turbulent kinetic energy are shown to differ significantly from their equilibrium flow variations.
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      The Structure of the Two-Dimensional Internal Boundary Layer over a Sudden Change of Surface Roughness

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152333
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    contributor authorRao, K. S.
    contributor authorWyngaard, J. C.
    contributor authorCoté, O. R.
    date accessioned2017-06-09T14:17:25Z
    date available2017-06-09T14:17:25Z
    date copyright1974/04/01
    date issued1974
    identifier issn0022-4928
    identifier otherams-16539.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152333
    description abstractThe effects of an abrupt change of surface roughness on the mean flow and turbulence structure in the neutral surface layer are numerically investigated by a higher-order turbulence closure theory, which includes dynamical equations for Reynolds stresses and the viscous dissipation rate. The closed system of governing equations, together with the specified initial and boundary conditions, is solved by an explicit finite-difference method on a digital computer. The numerical model predicts the distributions of mean wind, shear stress, turbulent energy and other quantities, with no a priori assumptions regarding the distributions of any of these variables in the transition region. The distributions of the nondimensional wind shear, the dissipation and mixing length scales, and the ratio of stress to turbulent kinetic energy are shown to differ significantly from their equilibrium flow variations.
    publisherAmerican Meteorological Society
    titleThe Structure of the Two-Dimensional Internal Boundary Layer over a Sudden Change of Surface Roughness
    typeJournal Paper
    journal volume31
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1974)031<0738:TSOTTD>2.0.CO;2
    journal fristpage738
    journal lastpage746
    treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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